Abstract. In this study, we present the technique of tunable diode laser
spectroscopy and the spectroscopic parameters of 13 lines of H2O in the 11980
-12260 cm−1 spectral region. Spectra were recorded at room temperature for a wide
range of pressures (2 - 15 Torr for pure H2O and 50 - 760 Torr for H2O in air). Line
parameters were adjusted from experiments using the least square method, Fortran
and three line-shape models: the Voigt profile (VP), the (hard collision) Rautian
profile (RP) and the speed dependent Voigt profile (SDVP). A comparison between
our results with the HITRAN database 2012 shows good agreement
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JOURNAL OF SCIENCE OF HNUE
Mathematical and Physical Sci., 2014, Vol. 59, No. 7, pp. 157-164
This paper is available online at
TUNABLE DIODE LASER SPECTROSCOPY AND LINE PARAMETERS
OF WATER VAPOR IN THE NEAR-INFRARED
Ngo Ngoc Hoa and Nguyen Manh Nghia
Faculty of Physics, Hanoi National University of Education
Abstract. In this study, we present the technique of tunable diode laser
spectroscopy and the spectroscopic parameters of 13 lines of H2O in the 11980
-12260 cm−1 spectral region. Spectra were recorded at room temperature for a wide
range of pressures (2 - 15 Torr for pure H2O and 50 - 760 Torr for H2O in air). Line
parameters were adjusted from experiments using the least square method, Fortran
and three line-shape models: the Voigt profile (VP), the (hard collision) Rautian
profile (RP) and the speed dependent Voigt profile (SDVP). A comparison between
our results with the HITRAN database 2012 shows good agreement.
Keywords:Water vapor, line-shape, tunable diode laser spectroscopy.
1. Introduction
Water vapor is a key molecule in the Earth’s atmosphere, its distribution the object
of several remote sensing experiments. The latter provide recordings of atmospheric
absorption spectra whose inversion yields the atmospheric humidity vertical profile. For
such applications, precise knowledge of the spectroscopic parameters of the H2O lines
is needed. In this work, line parameters (position, integrated intensity and broadening
coefficient) are deduced from laboratory spectra assuming a specific line-shape. For this,
the Voigt profile [1] is used in most of the available studies. Within this model, two
collisional parameters are used, i.e. the Lorentz broadening and shifting coefficients, the
Doppler width being fixed to its theoretical value. As is well known, [2-4], the Voigt
model can lead to discrepancies with measured spectra since it does not take into account
two velocity effects: (a) collision-induced velocity changes, leading to the so-called Dicke
narrowing and (b) the speed dependence of the pressure-induced width and shift. Using
more refined models that take into account such effects, several studies showed that the
line broadening determined by the Voigt profile can be underestimated up to 10% [2, 4]
while the error for integrated intensity is from 0.3 to 2% [5, 6].
Received August 12, 2014. Accepted October 13, 2014.
Contact Ngo Ngoc Hoa, e-mail address: hoa.nn@hnue.edu.vn
157
Ngo Ngoc Hoa and Nguyen Manh Nghia
Three spectral shape models have been used: the Voigt, the Rautian (to take into
account the Dicke narrowing effect) and the speed dependent Voigt models (to take
into account the speed dependence of the collisional parameters). The corresponding
absorption coefficients for a single line are given by [7]:
αV (σ) =
S.PH2O√
π
√
ln2
ΓD
Re {W (σ − σ0,ΓD,∆,Γ)} , (1.1)
αRP (σ) =
S.PH2O√
π
√
ln2
ΓD
Re
{
W (σ − σ0,ΓD,∆,Γ + B)
1−√πBW (σ − σ0,ΓD,∆,Γ + B)
}
, (1.2)
αSDV P (σ) =
S.PH2O
π3/2
√
ln2
ΓD
Im
+∞
∫
−∞
e−t
2
[1− Z ′(t)]
(σ − σ0)
√
ln2
ΓD
− t− Z(t)
dt
, (1.3)
where PH2O is the partial pressure of H2O and S is the integrated intensity of the line. σ0
and ΓD are the unperturbed spectral position of the transition, and the Doppler width Γ,
△ and B are the collisional half-width (HWHM), the pressure induced line-shift, and the
narrowing parameter, respectively. The complex probability function W is given by:
W (σ − σ0,ΓD,∆,Γ) = i
π
+∞
∫
−∞
e−t
2
(σ − σ0 −△)
√
ln2
ΓD
− t+ iΓ
√
ln2
ΓD
dt. (1.4)
The function Z(t) and its derivative Z’(t) in equation (3) are given by:
Z (t) =
√
ln2
ΓD
[∆ (v˜t) + Γ (v˜t)] , (1.5)
Z ′ (t) = v˜
√
ln2
ΓD
[
∆
′
(v˜t) + Γ
′
(v˜t)
]
, (1.6)
where v˜ is the most probable speed, △ (v˜t) and Γ(v˜t) being the speed dependent line
shifting and broadening parameters. The speed dependence of the line broadening is
modeled using a quadratic function [8].
2. Content
2.1. Experimental setup
The experimental setup used for the measurements of spectroscopic parameters of
water vapor in the near-infrared spectral region is shown in Figure 1. An external-cavity
158
Tunable diode laser spectroscopy and line parameters of water vapor in the near-infrared
diode laser [9] provides a wide tuning range of about 850 nm at room temperature. The
diode laser wavelength can be continuously scanned by means of a voltage-ramp signal
that simultaneously drives the laser injection current and the piezoelectric transducer that
sets the angle of the external-cavity grating. The emission line width of the diode laser is
about 1 MHz. In this spectral region, we investigated lines of the 2ν1 + ν2 + ν3 bands of
H2 16O by scanning intervals about 0.8 cm−1.
Figure 1. Experimental setup used for the measurements of line parameters
in the near-infrared region
A White blood cell with a total optical path of 40 m was used. The experiments
were carried out as follows: a spectrum was first recorded with the empty cell, providing
the 100% transmission reference. The cell was then filled with H2O vapor at pressures
ranging from 2 to 15 Torr, well below the saturated vapor pressure (about 18 Torr at
room temperature) and self-broadening spectra were recorded. For air-broadening spectra,
the cell was first filled with pure H2O (from 4 to 7 Torr) before ambient air was added
up to total pressures of 50 to 760 Torr. Partial pressures of H2O in the mixtures were
159
Ngo Ngoc Hoa and Nguyen Manh Nghia
then calculated using the integrated intensity determined from the pure H2O spectra. All
measurements in this study are realized by diode laser system at Paris East University.
A Fabry-Perot cavity was used for the calibration of the wavenumber scale. Two
spherical mirrors have a curvature radius of 75 mm, resulting in a free spectral range of 1
GHz (Figure 2). The finesse is 1000 leading to a resolution of 1 MHz. The peak positions
of this Fabry-Perot etalon allow a determination of the relative frequency scale with a
precision of better than 1 MHz (or 3.3.10−5 cm−1) while scanning the diode laser. The
peak positions of the Fabry Perot cavity were calibrated to relative wave numbers by using
a third degree polynomial function.
Figure 2. An example of the signal by recording simultaneously the detector signal,
the current ramp and the Fabry-Perot signal
2.2. Results and discussions
The measured spectra were least-squares fitted with the three profiles described
above and Doppler widths fixed to theoretical values. The integrated intensity, the
effective line position, and the line-shape parameters (Γ, B, Γ2), together with two
parameters describing the zero absorption level, are adjusted in the fits. As expected and
exemplified by Figure 3, the VP leads to significant residuals, and the RP and SDVP are
in better agreement with measured spectra.
The three lowest panels show the differences between measured absorptions and
those adjusted using the VP, RP and SDVP.
160
Tunable diode laser spectroscopy and line parameters of water vapor in the near-infrared
Figure 3. Room temperature measured absorptions
of the 606 ← 505 (12249.3895 cm−1) transition
of pure water vapor (left) and of H2O in air (right) at different pressures
2.2.1. Integrate intensities
For the integrated intensity, only the results from pure H2O spectra were used. As
can be seen from this table and Figure 4, the RP and the SDVP lead to very close values,
both slightly larger (typically by 0.8%) than those determined with the VP. This result is
fully consistent with those obtained in other spectral regions [5, 6].
Figure 4. Ratios of the intensities of the 13 considered transitions obtained
by the RP (◦) and SDVP () to those obtained by the VP
2.2.2. Broadening coefficients
The self-broadening coefficients were determined from fits of pure H2O spectra,
shown in Figure 5a, display the collisional line-widths of the transition at 12249.3895
cm−1, which shows that they have the expected linear variation with the H2O pressure.
The slopes give broadening coefficients. For example with the transition at 12249.3895
cm−1, the corresponding broadening coefficients obtained with the VP, RP and SDVP are
161
Ngo Ngoc Hoa and Nguyen Manh Nghia
0.429, 0.446 and 0.452 cm−1.atm−1, respectively. The smaller value obtained with the VP
shows the effect of the line narrowing, observed in Figure 3. For spectra of H2O diluted
in ambient air, the total line-width of a transition is written as:
Γ = γself .PH2O + γair. (P − PH2O) ,
where γself and γair are the self and air-broadening coefficients, respectively. P is the total
pressure in the celle. In order to determine γair, the partial pressure PH2O in the cell was for
each spectrum first determined from the ratio of the integrated area under the measured
spectrum (obtained from fits) to the line intensity determined from the spectrum of pure
H2O. A linear fit of (Γ− γself.PH2O) versus Pair = (P - PH2O) gives γair. As exemplified in
Figure 5b, the values obtained vary linearly with Pair. The slopes from Figure 5b (0.0763,
0.0792 and 0.0799 cm−1.atm−1 obtained with the VP, RP and SDVP, respectively) again
demonstrate the consistency of the RP and SDVP determinations and the underestimation
of the broadening by the VP of about 5% as presented in Figure 6.
Figure 5. Line widths of the transition at 12249.3895 cm−1 as functions
of (a) the H2O pressure and (b) air pressure,
obtained using the VP, RP and SDVP
Figure 6. Ratios of (a) the self and (b) the air-broadening coefficients
of the 13 considered transitions obtained
using the SDVP () and the RP(◦) to those obtained using the VP
162
Tunable diode laser spectroscopy and line parameters of water vapor in the near-infrared
The H2O vapor self- and air-broadening coefficients from this study obtained using
the VP are compared with data from the literature HITRAN08 [10] and HITRAN12 [11].
Note that our results are in good agreement with all previous studies as shown in Table 1
and Figure 7. The self-broadening coefficients from this study are slightly lower than the
values in the databases with a mean deviation of 2% and 7%. However, the air-broadening
coefficients are about 4% higher than the values in the databases.
Table 1. H2O self and air-broadening coefficients at 296 K
S,
0, cm−1
10−23 cm−1
molec−11 cm2
self, cm
−1 atm−1
air, cm−1 atm−1
VP VP [10] [11] VP [10] [11]
11988.4939 1.0626 0.369 0.353 0.352 0.0681 0.0708 0.0708
11988.7257 0.3422 0.314 0.364 0.352 0.0654 0.0742 0.0742
12226.1012 4.8473 0.526 0.461 0.483 0.0931 0.0933 0.0954
12236.5601 4.0128 0.475 0.416 0.412 0.0850 0.0842 0.0849
12244.7186 3.5084 0.467 0.424 0.398 0.0899 0.0952 0.0958
12244.7881 1.0197 0.392 0.299 0.402 0.0694 0.0681 0.0681
12248.5787 0.9492 0.362 0.352 0.391 0.0703 0.0754 0.0774
12249.3895 2.6468 0.429 0.376 0.391 0.0763 0.0773 0.0776
12259.4776 0.5645 0.354 0.323 0.313 0.0665 0.0691 0.0673
12259.6033 1.6060 0.358 0.330 0.348 0.0627 0.0621 0.0621
12268.9969 1.0111 0.300 0.258 0.352 0.0530 0.0618 0.0618
12280.4387 0.2820 0.389 0.429 0.421 0.0754 0.0801 0.0801
12280.6634 0.9262 0.374 0.329 0.343 0.0719 0.0725 0.0725
Figure 7. A comparison of the H2O self- and air-broadening parameter
from the present work with those from other studies [10, 11]
as a function of line intensity
163
Ngo Ngoc Hoa and Nguyen Manh Nghia
3. Conclusion
Absorption spectra of 13 lines of H2O in the near infrared spectral were recorded at
room temperature using a tunable diode laser system. Line parameters were determined
from experiments using three line-shape models: the Voigt profile (VP), the (hard
collision) Rautian profile (RP) and the speed dependent Voigt profile (SDVP). The results
show that the RP and SDVP are in better agreement with measurements than the VP and
that they lead to larger values of the line parameters (about 5% for the line broadening and
0.8% for line intensity). The comparison between our results and the HITRAN database
2008 and 2012 shows good agreement.
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